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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;L354&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Limestone, shelly&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Middle Jurassic&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Forest Marble&lt;br /&gt;Near Weymouth&lt;/div&gt;
&lt;/div&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;This rock is made up of well cemented bioclasts. The bioclasts (mainly shell fragments) are poorly sorted, ranging from &amp;lt;1mm up to a few 10s of mm.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Fine-grained cement fizzes with acid, indicating that it is carbonate. It has weathered to a pale yellow-grey.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;Carbonate fossil fragment in a carbonate cement (sparite). The laminated structure of the shells is visible in places.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Cement contains some hematite (brown regions).&lt;span&gt; &lt;/span&gt;&lt;br /&gt;There are a few epidote grains and some opaque areas.&lt;br /&gt;This is a rudstone (Dunham naming system) or biosparite (Folk naming system).&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;The shells are not in life position – they have been transported.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Deposited in moderate to high energy environment.&lt;span&gt; &lt;/span&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;shelly limestone&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>bioclastic</name>
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        <name>biosparite</name>
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        <name>high energy</name>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;L311&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Conglomerate&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Eocene&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Hertfordshire&lt;/div&gt;
&lt;/div&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;div class="element-set"&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Hand Specimen&lt;/h3&gt;
&lt;div class="element-text"&gt;Poorly sorted. Rounded clasts up to ~15 mm long.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Pale yellow matrix of quartz grains.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Cement fizzes with acid, indicating that it contains carbonate.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;This conglomerate is just clast-supported.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Thin-section&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Rounded clasts of very dark red brown&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/171"&gt;amorphous&lt;/a&gt;&lt;span&gt; &lt;/span&gt;silica (chert) and&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/242"&gt;polycrystalline&lt;/a&gt; quartz.&lt;/p&gt;
&lt;p&gt;Matrix of quartz grains (typically 0.25 mm) and fine-grained carbonate cement (sparite). Dark red-brown&lt;span&gt; &lt;/span&gt;&lt;span&gt;iron staining&lt;/span&gt;.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;Deposited in a high energy environment.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced Notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;span&gt;Iron staining&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Hematite (Fe&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;3&lt;/sub&gt;) → red (blood-red, cherry-red, brown-red) iron-staining&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Limonite (FeO(OH)•nH&lt;sub&gt;2&lt;/sub&gt;O) → yellow or brown iron-staining&lt;/p&gt;
&lt;p&gt;The red-brown colour of this rock is probably produced by hematite.&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Name&lt;/h3&gt;
&lt;div class="element-text"&gt;conglomerate&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>clast supported</name>
      </tag>
      <tag tagId="38">
        <name>high energy</name>
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